Study of spatial distribution of sandy desertification in North China in recent 10 years
Sandy desertification is a land degradation characterized by wind erosion, mainly resulted from the excessive human activities in arid, semiarid and part of sub-humid regions in North China. It is one of main kinds of desertification/land degradation as well as water-soil erosion and salinization in...
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| Veröffentlicht in: | Science China. Earth sciences 2004-01, Vol.47 (S1), p.78-88 |
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| creator | Wang, Tao Wu, Wei Xue, Xian Sun, Qingwei Chen, Guangting |
| description | Sandy desertification is a land degradation characterized by wind erosion, mainly resulted from the excessive human activities in arid, semiarid and part of sub-humid regions in North China. It is one of main kinds of desertification/land degradation as well as water-soil erosion and salinization in China. Rapid and continuous spread of sandy desertification during last 50 years has created a major environmental and socio-economic problem in North China. Remote sensing monitored results in 2000 showed that the sandy desertified land area has been 38.57 × 104 km2. The area of potential to slightly sandy desertified land is 13.93 × 104 km2, moderately land 9.977 ×104 km2, severely land 7.909 × 104 k2 and very severely land 6.756 × 104 km2. Sandy desertification mainly occurs in the semi-arid mixed farming-grazing zone and its northern rangeland zone, semi-arid dryland rainfed cropping zone and arid oasis-desert margin zone. The average annually developmental rate of sandy desertified land increased from 2,100 km2 · a-1 in 1976–1988 to 3,600 km2 · a-1 in 1988–2000. The basic status of sandy desertification in North China is “overall deterioration, while local rehabilitation”. Already achieved rehabilitation results and monitoring assessment show that about 60% of desertified land in North China can be restored under the conditions of rational land-use ways and intensity. |
| doi_str_mv | 10.1360/04zd0009 |
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It is one of main kinds of desertification/land degradation as well as water-soil erosion and salinization in China. Rapid and continuous spread of sandy desertification during last 50 years has created a major environmental and socio-economic problem in North China. Remote sensing monitored results in 2000 showed that the sandy desertified land area has been 38.57 × 104 km2. The area of potential to slightly sandy desertified land is 13.93 × 104 km2, moderately land 9.977 ×104 km2, severely land 7.909 × 104 k2 and very severely land 6.756 × 104 km2. Sandy desertification mainly occurs in the semi-arid mixed farming-grazing zone and its northern rangeland zone, semi-arid dryland rainfed cropping zone and arid oasis-desert margin zone. The average annually developmental rate of sandy desertified land increased from 2,100 km2 · a-1 in 1976–1988 to 3,600 km2 · a-1 in 1988–2000. The basic status of sandy desertification in North China is “overall deterioration, while local rehabilitation”. Already achieved rehabilitation results and monitoring assessment show that about 60% of desertified land in North China can be restored under the conditions of rational land-use ways and intensity.</description><identifier>ISSN: 1006-9313</identifier><identifier>ISSN: 1674-7313</identifier><identifier>EISSN: 1862-2801</identifier><identifier>EISSN: 1869-1897</identifier><identifier>DOI: 10.1360/04zd0009</identifier><language>eng</language><publisher>Dordrecht: Springer Nature B.V</publisher><subject>Arid lands ; Arid regions ; Arid zones ; Aridity ; Assessments ; China ; Degradation ; Desertification ; Environmental degradation ; Erosion ; Land ; Land degradation ; Land use ; Mixed cropping ; Oases ; Rangelands ; Rehabilitation ; Remote monitoring ; Remote sensing ; Salinization ; Semiarid zones ; Socioeconomic aspects ; Soil erosion ; Soil water ; Spatial distribution ; Spreads ; Wind erosion</subject><ispartof>Science China. Earth sciences, 2004-01, Vol.47 (S1), p.78-88</ispartof><rights>Science in China Press 2004.</rights><rights>Science in China Press 2004</rights><rights>Copyright © Wanfang Data Co. Ltd. All Rights Reserved.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a368t-bb907ee0fea7dc557275f76c391f5ef5a54581a328dac5e61a7982050e772dad3</citedby><cites>FETCH-LOGICAL-a368t-bb907ee0fea7dc557275f76c391f5ef5a54581a328dac5e61a7982050e772dad3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Uhttp://www.wanfangdata.com.cn/images/PeriodicalImages/zgkx-ed/zgkx-ed.jpg</thumbnail><link.rule.ids>314,776,780,27901,27902</link.rule.ids></links><search><creatorcontrib>Wang, Tao</creatorcontrib><creatorcontrib>Wu, Wei</creatorcontrib><creatorcontrib>Xue, Xian</creatorcontrib><creatorcontrib>Sun, Qingwei</creatorcontrib><creatorcontrib>Chen, Guangting</creatorcontrib><title>Study of spatial distribution of sandy desertification in North China in recent 10 years</title><title>Science China. Earth sciences</title><description>Sandy desertification is a land degradation characterized by wind erosion, mainly resulted from the excessive human activities in arid, semiarid and part of sub-humid regions in North China. It is one of main kinds of desertification/land degradation as well as water-soil erosion and salinization in China. Rapid and continuous spread of sandy desertification during last 50 years has created a major environmental and socio-economic problem in North China. Remote sensing monitored results in 2000 showed that the sandy desertified land area has been 38.57 × 104 km2. The area of potential to slightly sandy desertified land is 13.93 × 104 km2, moderately land 9.977 ×104 km2, severely land 7.909 × 104 k2 and very severely land 6.756 × 104 km2. Sandy desertification mainly occurs in the semi-arid mixed farming-grazing zone and its northern rangeland zone, semi-arid dryland rainfed cropping zone and arid oasis-desert margin zone. The average annually developmental rate of sandy desertified land increased from 2,100 km2 · a-1 in 1976–1988 to 3,600 km2 · a-1 in 1988–2000. The basic status of sandy desertification in North China is “overall deterioration, while local rehabilitation”. Already achieved rehabilitation results and monitoring assessment show that about 60% of desertified land in North China can be restored under the conditions of rational land-use ways and intensity.</description><subject>Arid lands</subject><subject>Arid regions</subject><subject>Arid zones</subject><subject>Aridity</subject><subject>Assessments</subject><subject>China</subject><subject>Degradation</subject><subject>Desertification</subject><subject>Environmental degradation</subject><subject>Erosion</subject><subject>Land</subject><subject>Land degradation</subject><subject>Land use</subject><subject>Mixed cropping</subject><subject>Oases</subject><subject>Rangelands</subject><subject>Rehabilitation</subject><subject>Remote monitoring</subject><subject>Remote sensing</subject><subject>Salinization</subject><subject>Semiarid zones</subject><subject>Socioeconomic aspects</subject><subject>Soil erosion</subject><subject>Soil water</subject><subject>Spatial distribution</subject><subject>Spreads</subject><subject>Wind erosion</subject><issn>1006-9313</issn><issn>1674-7313</issn><issn>1862-2801</issn><issn>1869-1897</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2004</creationdate><recordtype>article</recordtype><sourceid>BENPR</sourceid><recordid>eNp1kV1LHDEUhgexULVCf8KgF_Zm7EkymSSXstgqSHvRFrwLZycnGl0za5Khrr--s2tVELw6Xw_n662qzwyOmejgK7SPDgDMVrXDdMcbroFtTz5A1xjBxMdqN-cbAGFka3aqy19ldKt68HVeYgm4qF3IJYX5WMIQN3mME-AoUyrBhx43hRDrH0Mq1_XsOkRch4l6iqVmUK8IU_5UffC4yLT_3-5Vf76d_p6dNRc_v5_PTi4aFJ0uzXxuQBGBJ1Sul1JxJb3qemGYl-QlylZqhoJrh72kjqEymoMEUoo7dGKv-vLU9y9Gj_HK3gxjitNE-3h1-2DJcZheMp1vJvToCV2m4X6kXOxdyD0tFhhpGLPVUrSaMcMn8uAN-dJVdVwa1rZqgg7fg7jSqpWdVPC6X5-GnBN5u0zhDtPKMrBrxeyzYuIfrLCGuw</recordid><startdate>20040101</startdate><enddate>20040101</enddate><creator>Wang, Tao</creator><creator>Wu, Wei</creator><creator>Xue, Xian</creator><creator>Sun, Qingwei</creator><creator>Chen, Guangting</creator><general>Springer Nature B.V</general><general>Key Laboratory of Desert and Desertification, Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou 730000, China%Department of Environment Engineering, Peking University, Beijing 100871, China</general><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7TG</scope><scope>7UA</scope><scope>7XB</scope><scope>88I</scope><scope>8FK</scope><scope>ABUWG</scope><scope>AEUYN</scope><scope>AFKRA</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>C1K</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>F1W</scope><scope>GNUQQ</scope><scope>H96</scope><scope>HCIFZ</scope><scope>KL.</scope><scope>L.G</scope><scope>M2P</scope><scope>PCBAR</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>Q9U</scope><scope>8FD</scope><scope>FR3</scope><scope>KR7</scope><scope>2B.</scope><scope>4A8</scope><scope>92I</scope><scope>93N</scope><scope>PSX</scope><scope>TCJ</scope></search><sort><creationdate>20040101</creationdate><title>Study of spatial distribution of sandy desertification in North China in recent 10 years</title><author>Wang, Tao ; Wu, Wei ; Xue, Xian ; Sun, Qingwei ; Chen, Guangting</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a368t-bb907ee0fea7dc557275f76c391f5ef5a54581a328dac5e61a7982050e772dad3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2004</creationdate><topic>Arid lands</topic><topic>Arid regions</topic><topic>Arid zones</topic><topic>Aridity</topic><topic>Assessments</topic><topic>China</topic><topic>Degradation</topic><topic>Desertification</topic><topic>Environmental degradation</topic><topic>Erosion</topic><topic>Land</topic><topic>Land degradation</topic><topic>Land use</topic><topic>Mixed cropping</topic><topic>Oases</topic><topic>Rangelands</topic><topic>Rehabilitation</topic><topic>Remote monitoring</topic><topic>Remote sensing</topic><topic>Salinization</topic><topic>Semiarid zones</topic><topic>Socioeconomic aspects</topic><topic>Soil erosion</topic><topic>Soil water</topic><topic>Spatial distribution</topic><topic>Spreads</topic><topic>Wind erosion</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Wang, Tao</creatorcontrib><creatorcontrib>Wu, Wei</creatorcontrib><creatorcontrib>Xue, Xian</creatorcontrib><creatorcontrib>Sun, Qingwei</creatorcontrib><creatorcontrib>Chen, Guangting</creatorcontrib><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Water Resources Abstracts</collection><collection>ProQuest Central (purchase pre-March 2016)</collection><collection>Science Database (Alumni Edition)</collection><collection>ProQuest Central (Alumni) (purchase pre-March 2016)</collection><collection>ProQuest Central (Alumni Edition)</collection><collection>ProQuest One Sustainability</collection><collection>ProQuest Central UK/Ireland</collection><collection>ProQuest Central Essentials</collection><collection>ProQuest Central</collection><collection>Natural Science Collection</collection><collection>Earth, Atmospheric & Aquatic Science Collection</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central Korea</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>ProQuest Central Student</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>SciTech Premium Collection</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Science Database</collection><collection>Earth, Atmospheric & Aquatic Science Database</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>ProQuest Central Basic</collection><collection>Technology Research Database</collection><collection>Engineering Research Database</collection><collection>Civil Engineering Abstracts</collection><collection>Wanfang Data Journals - Hong Kong</collection><collection>WANFANG Data Centre</collection><collection>Wanfang Data Journals</collection><collection>万方数据期刊 - 香港版</collection><collection>China Online Journals (COJ)</collection><collection>China Online Journals (COJ)</collection><jtitle>Science China. Earth sciences</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Wang, Tao</au><au>Wu, Wei</au><au>Xue, Xian</au><au>Sun, Qingwei</au><au>Chen, Guangting</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Study of spatial distribution of sandy desertification in North China in recent 10 years</atitle><jtitle>Science China. Earth sciences</jtitle><date>2004-01-01</date><risdate>2004</risdate><volume>47</volume><issue>S1</issue><spage>78</spage><epage>88</epage><pages>78-88</pages><issn>1006-9313</issn><issn>1674-7313</issn><eissn>1862-2801</eissn><eissn>1869-1897</eissn><abstract>Sandy desertification is a land degradation characterized by wind erosion, mainly resulted from the excessive human activities in arid, semiarid and part of sub-humid regions in North China. It is one of main kinds of desertification/land degradation as well as water-soil erosion and salinization in China. Rapid and continuous spread of sandy desertification during last 50 years has created a major environmental and socio-economic problem in North China. Remote sensing monitored results in 2000 showed that the sandy desertified land area has been 38.57 × 104 km2. The area of potential to slightly sandy desertified land is 13.93 × 104 km2, moderately land 9.977 ×104 km2, severely land 7.909 × 104 k2 and very severely land 6.756 × 104 km2. Sandy desertification mainly occurs in the semi-arid mixed farming-grazing zone and its northern rangeland zone, semi-arid dryland rainfed cropping zone and arid oasis-desert margin zone. The average annually developmental rate of sandy desertified land increased from 2,100 km2 · a-1 in 1976–1988 to 3,600 km2 · a-1 in 1988–2000. The basic status of sandy desertification in North China is “overall deterioration, while local rehabilitation”. Already achieved rehabilitation results and monitoring assessment show that about 60% of desertified land in North China can be restored under the conditions of rational land-use ways and intensity.</abstract><cop>Dordrecht</cop><pub>Springer Nature B.V</pub><doi>10.1360/04zd0009</doi><tpages>11</tpages></addata></record> |
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| ispartof | Science China. Earth sciences, 2004-01, Vol.47 (S1), p.78-88 |
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| source | Alma/SFX Local Collection; SpringerLink Journals - AutoHoldings |
| subjects | Arid lands Arid regions Arid zones Aridity Assessments China Degradation Desertification Environmental degradation Erosion Land Land degradation Land use Mixed cropping Oases Rangelands Rehabilitation Remote monitoring Remote sensing Salinization Semiarid zones Socioeconomic aspects Soil erosion Soil water Spatial distribution Spreads Wind erosion |
| title | Study of spatial distribution of sandy desertification in North China in recent 10 years |
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